Characterization of Atmospheric Aerosol over XiAn in the South Margin of the Loess Plateau, China

2002 ◽  
Vol 36 (26) ◽  
pp. 4189-4199 ◽  
Author(s):  
Xiao Y Zhang ◽  
J.J Cao ◽  
L.M Li ◽  
R Arimoto ◽  
Y Cheng ◽  
...  
2018 ◽  
Author(s):  
Ze Min Ai ◽  
Jiao Yang Zhang ◽  
Hong Fei Liu ◽  
Sha Xue ◽  
Guo Bin Liu

Abstract. Slope aspect is an important topographic factor, but its effect on the microbial properties of grassland rhizospheric soil (RS) and non-rhizospheric soil (NRS) remain unclear. A field experiment was conducted at the Ansai Research Station on the Loess Plateau in China to test the influence of slope aspects (south-facing, north-facing, and northeast-facing slopes, all with Artemisia sacrorum as the dominant species) on RS and NRS microbial biomass carbon (MBC) and phospholipid fatty acid (PLFA) contents, and the rhizospheric effect (RE) of various microbial indices. MBC content differed significantly among the slope aspects in RS but not in NRS, and RE for MBC content in the south-facing slope was larger than that in the north-facing slope. RS total, bacterial, and gram-positive bacterial PLFA contents in the south-facing slope were significantly lower than those in the north- and northeast-facing slopes, and RS gram-negative bacterial (G-) and actinomycete PLFA contents in the south-facing slope were significantly lower than those in the north-facing slope. Differently, NRS total, bacterial, and G- PLFA contents in the north-facing slope were significantly higher than those in the south- and northeast-facing slopes, and NRS fungal and actinomycete PLFA contents in the north- and south-facing slopes were significantly higher than those in the northeast-facing slope. RE for all PLFA contents except fungal in the northeast-facing slope were higher than those in the south-facing slope. Slope aspect significantly but differentially affected the microbial properties in RS and NRS, and the variable influence was due an evident RE for most microbial properties.


2019 ◽  
Vol 11 (2) ◽  
pp. 228-240 ◽  
Author(s):  
Chunlei Zhao ◽  
Ming’an Shao ◽  
Xiaoxu Jia ◽  
Laiming Huang ◽  
Yuanjun Zhu

2014 ◽  
Vol 5 (3) ◽  
pp. 421-430 ◽  
Author(s):  
Qian Zhang ◽  
Zhenxing Shen ◽  
Junji Cao ◽  
KinFai Ho ◽  
Renjian Zhang ◽  
...  

Solid Earth ◽  
2018 ◽  
Vol 9 (5) ◽  
pp. 1157-1168 ◽  
Author(s):  
Ze Min Ai ◽  
Jiao Yang Zhang ◽  
Hong Fei Liu ◽  
Sha Xue ◽  
Guo Bin Liu

Abstract. Slope aspect is an important topographic factor in the micro-ecosystem environment, but its effect on the microbial properties of grassland rhizospheric soil (RS) and non-rhizospheric soil (NRS) remain unclear. A field experiment was conducted at the Ansai Research Station on the Loess Plateau in China to test the influence of slope aspects (south-facing, north-facing, and northwest-facing slopes, all with Artemisia sacrorum as the dominant species) on RS and NRS microbial biomass carbon (MBC) contents, phospholipid fatty acid (PLFA) contents, and the rhizospheric effect (RE) of various microbial indices. Soil samples were collected from the three slope aspects, including rhizospheric and non-rhizospheric region, and analyzed to determine the various related microbial indices. The results showed that MBC content differed significantly among the slope aspects in RS but not in NRS, and the RE for MBC content in the south-facing slope was larger than that in the north-facing slope. RS total, bacterial, and Gram-positive bacterial PLFA contents in the south-facing slope were significantly lower than those in the north- and northwest-facing slopes, and RS Gram-negative bacterial (G−) and actinomycete PLFA contents in the south-facing slope were significantly lower than those in the north-facing slope. In contrast, NRS total, bacterial, and G− PLFA contents in the north-facing slope were significantly higher than those in the south- and northwest-facing slopes, and NRS fungal and actinomycete PLFA contents in the north- and south-facing slopes were significantly higher than those in the northwest-facing slope. RE for all PLFA contents except fungal in the northwest-facing slope were higher than those in the south-facing slope. Slope aspect significantly but differentially affected the microbial properties in RS and NRS, and the variable influence was due to an evident RE for most microbial properties.


2019 ◽  
Vol 80 (9) ◽  
pp. 1796-1806 ◽  
Author(s):  
Tiantian Shao ◽  
Tao Wang ◽  
Xiaowen Liang ◽  
Honglian Xu ◽  
Liuyang Li

Abstract Dissolved organic carbon (DOC) and chromophoric dissolved organic matter (CDOM) in rivers and reservoirs on the western Loess Plateau, which is an area of severe soil erosion, were investigated in September 2017 to analyze the CDOM characteristics and composition, DOC distribution and influence of environmental factors on these parameters. Great differences of water parameters were exhibited between different groups based on the analysis of variance (p < 0.01). The results indicated that rivers exhibited higher DOC concentrations (mean: 3.70 mg/L) than reservoir waters (mean: 2.04 mg/L). Artificial and agricultural lands exert a large influence on DOC concentrations, which verifies the hypothesis that intense anthropogenic activity results in high DOC concentrations. The CDOM absorption at 350 nm [aCDOM(350)] of tributary water samples was 2.73 m−1, which was higher than that in the Yellow River (1.71 m−1) and reservoir waters (1.33 m−1). The effects of DOC, TC and turbulence (Tur) on CDOM are positive and significant (p < 0.05) according to the multiple linear regressions. An analysis of the optical characteristics of CDOM indicated that waters on the Loess Plateau contained abundant humic acid and higher levels of allochthonous DOM with a higher molecular weight (MW) based on the spectral slopes (S) and specific UV absorbance (SUVA254) values.


2009 ◽  
Vol 29 (1) ◽  
pp. 103-108
Author(s):  
Jianming LIANG ◽  
Jie ZHOU ◽  
Zhong HE ◽  
Weiguo LIU ◽  
Yinli LIANG ◽  
...  

2015 ◽  
Vol 117 ◽  
pp. 212-219 ◽  
Author(s):  
Pengfei Tian ◽  
Xianjie Cao ◽  
Lei Zhang ◽  
Hongbin Wang ◽  
Jinsen Shi ◽  
...  

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